The spatial and temporal characteristics of the month-to-month variability
of the polar night jet and its relationship with tropospheric circulation i
s investigated for both the Northern and Southern Hemispheres. The variabil
ities of the hemispheres have many common characteristics of the Polar Nigh
t Jet Oscillation (PJO). These common characteristics include the following
: (1) the anomalous zonal-mean zonal winds shift poleward and downward; (2)
the anomalous polar temperatures propagate downward from the stratopause t
o the upper troposphere; and (3) they are made through a wave-mean flow int
eraction with mainly the planetary wave of zonal wave number one. Annular m
odes associated with the PJOs appear in both hemispheres when the zones of
maximum polar temperature anomaly descend to the lowermost stratosphere and
upper troposphere. The major difference in the PJOs of the two hemispheres
is found in their temporal characteristics. In the Southern Hemisphere, th
e phase of the PJO is closely locked to the annual cycle, while in the Nort
hern Hemisphere it exhibits quasiperiodic variability with its envelope con
trolled by the annual cycle. The origin of the differences between the PJOs
is discussed based on the theory of the wave-mean flow interaction.